Abstract

This paper presents a comparison between two procedures for the generation of water demand time series at both single user and nodal scales, a top-down and a bottom-up procedure respectively. Both procedures are made up of two phases. The top-down procedure adopted includes a non-parametric disaggregation based on the K-nearest neighbours approach. Therefore, once the temporal aggregated water demand patterns have been defined (first phase), the disaggregation is used to generate water demand time series at lower levels of spatial aggregation (second phase). In the bottom-up procedure adopted, demand time series for each user and for each time step are generated applying a beta probability distribution with tunable bounds or a gamma distribution with shift parameter (first phase). Then, a Copula based re-sort is applied to the demand time series generated to impose existing rank cross-correlations between users and at all temporal lags (second phase). For the sake of comparison, two case studies were considered, both of which are related to a smart water network in Naples (Italy). The results obtained show that the bottom-up procedure performs significantly better than the top-down procedure in terms of rank-cross correlations at fine scale. However, the top-down procedure showed a better performance in terms of skewness and rank cross-correlation when the aggregated demands were considered. Finally, the level of aggregation in nodes was found to affect the performance of both the procedures considered.

Highlights

  • Accurate estimates of nodal demands are of fundamental importance for numerical simulation of water distribution networks (WDNs) behavior

  • This paper presents a comparison between two procedures for the generation of water demand time series at both single user and nodal scales, a top-down and a bottom-up procedure respectively

  • In its most common deterministic application, once the water demand pattern has been defined at high levels of spatial aggregation, the nodal water demand patterns are usually obtained by disaggregating the total amount of water supplied in proportion to the average demand at each node

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Summary

Introduction

Accurate estimates of nodal demands are of fundamental importance for numerical simulation of water distribution networks (WDNs) behavior. In its most common deterministic application, once the water demand pattern has been defined at high levels of spatial aggregation, the nodal water demand patterns are usually obtained by disaggregating the total amount of water supplied in proportion to the average demand at each node. This approach does not consider both the random character of water demands and their variability. The importance of taking into account the variability of water demands was highlighted by several studies [3,4,5,6]

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